Mesoscale (METR 4433) Spring 2015 Study Guide for Hour Exam #2

The following is intended to serve as a general guide for your exam preparation, and is not necessarily all inclusive. Questions one all aspects covered in the lectures are possible.

Single Cell

 Know the definition of a thunderstorm.  Understand the classification system of thunderstorms, the characteristics of single cells, multicells, lines and , and the principal differences in environmental conditions among them.  Understand the concept of water loading and how it contributes to updraft acceleration/deceleration.  Understand the concept of CAPE and how it relates to updraft acceleration. Be sure you understand the approximations associated with relating the two.  Be able to compute the CAPE and Wmax (via integration) if given an appropriate expression for buoyancy.  Understand how CAPE is represented on a thermodynamic diagram.  Understand and be able to explain convective inhibition (CIN) and its role in promoting or inhibiting moist convection.  Be able to explain mechanisms by which CAPE and CIN can increase or decrease.  Know the principal ingredients needed for thunderstorms to form and the role of environmental shear.  Be able to define and apply the bulk Richardson number to determine classification.  Understand and be able to explain the characteristics and life cycle of single-cell storms, including the built-in self-destruct mechanism.  Understand the origin and forcing mechanisms (entrainment, water loading, evaporation) for storm downdrafts.  Be able to explain the cold-air outflow and the importance of the gust front.  Be able to define microbursts and explain their origin and structure.  Be able to explain the differences between wet and dry microbursts.  Be able to explain why microbursts pose a hazard to aviation, using graphics to back up your arguments for an airplane on takeoff or landing.  Be able to describe, in general, the systems now in place to detect and predict microbursts.

1 Multicell Storms

 Understand the characteristics of multicellular storms and how they differ from isolated, single cell storms.  Be able to explain the environmental conditions that are conducive to the formation of multicell storms.  Know the types of typically associated with multicell storms.  Be able to explain the life cycle of a classic multicellular storm.  Understand the mechanisms of multicell propagation/movement and how cell motion influences storm system motion.  Understand the vorticity dynamics of cold-air outflows and be able to explain the flow pattern behind the gust front  Understand how an integral of the equations of motion can be used to estimate gust front propagation speed and be able to explain the physical mechanism by which gust fronts/cold outflows propagate.  Be able to explain the presence of turbulence atop a cold outflow including the association pressure perturbations and their possible influence on gust front propagation speed.  Understand why a pressure jump occurs in the environment ahead of a propagating gust front.  Be able to draw a schematic of a cold outflow/gust front system and explain the importance of the flow.  Be able to describe the life cycle of cells triggered along the gust front in a multicell storm system and the manner in which updrafts and downdrafts either work together or in competition.

Bright Bands.

 The phenomena, and reason that they exist.

Bow Echoes

 The phenomena and weather.  The conceptual model, typical life cycle of bow echoes, and the stages that typical bow echoes evolves though.  Bookend vortices, their origin and their impact on low-level circulation and surface  Rear inflow notch and its association with rear inflow jet.  Favorable environment for severe bow echoes  Derechoes and their forms and weather

2 Mesoscale Convective Complexes

 Definition and significant weather  The typical structure and evolution

Squall lines

 General characteristics of lines  Conceptual models of squall lines  Flow pattern in mature squall lines  Weather associated with mature squall lines  Different ways forms  Effect of vertical shear on long-lasting squall lines  Behaviors and evolutions of squall lines forming in environmental shear of different strength  Perturbation pressure patterns associated with squall lines and their cause and effect  Effect of vorticity sources on the evolution of squall lines  Rotunno, Klemp and Weisman's views of the role of low-level shear and cold in long lived squall lines  RKW's Optimal condition for long-lasting squall lines

Supercell Storms

storm, definition, typical weather  Types of supercell storms, LP, HP and classic supercell storms  Supercell characteristics, typical internal flow structure, main branches of flow, roles and behaviors of updraft and downdraft  Typical echo patterns of supercell storm in both horizontal and vertical plane views and the causes of such patterns  Wall clouds and processes by which they form

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